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The relationship between past vegetation type and fire frequency in western Japan inferred from phytolith and charcoal records in cumulative soils

机译:根据累积土壤中的植物石炭和木炭记录推断的日本西部过去植被类型与火灾频率之间的关系

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Phytolith and macrocharcoal records in cumulative soils were compared in five areas in western Japan, including two sites on the Tonomine Plateau where we examined those records. Past vegetation types, as represented by the compositions of phytolith assemblages, are closely related to macrocharcoal fluxes, regardless of age, suggesting that in Japan, fluxes in cumulative soils could be an indicator of fire frequency. On the Tonomine Plateau, phytolith and charcoal records indicate that, in the middle and late Holocene (at least 5000 to similar to 1000 years ago), Sasa and Panicoideae species in a temperate climate. At least for approximately the last 600 years the Japanese pampas (Miscanthus sinensis) grassland has undergone annual burning. The results from the Tonomine Plateau site of this study and from four other sites suggest that macrocharcoal fluxes in cumulative soils of > 10 particles.cm(-2) y(-1) indicate a high frequency of fires, resulting in the dominance of Andropogoneae species. Dominance of Pleioblastus species under the influence of fire was observed in soils with a charcoal flux of 2-10 particles.cm(-2) y(-1), suggesting that the species flourished under a moderate frequency of fire (possibly every several years or more). In soils with a charcoal flux of less than similar to 1 particles.cm(-2) y(-1), there was no influence of fire on vegetation, and Sasa and Pleioblastus species flourished where the vegetation type was determined primarily by the climatic conditions. These findings indicate that macrocharcoal fluxes and phytolith assemblages exhibit a consistent relationship that is independent of age, and that macrocharcoal fluxes are linked to fire frequency, thus suggesting that the frequency of fire has determined the vegetation type in these areas. Therefore, phytolith and charcoal records in cumulative soils provide a context for quantitatively understanding the influence of fire on vegetation patterns in the past. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:在日本西部的五个地区(包括在Tonomine高原的两个地点)中,我们比较了累积土壤中的植硅石和大型木炭记录,我们检查了这些记录。以植物石器组合物的成分为代表的过去的植被类型与宏观碳通量密切相关,而不论其年龄如何,这表明在日本,累积土壤中的通量可能是火灾发生频率的指标。在Tonomine高原上,植硅石和木炭记录表明,在全新世的中晚期(至少5000到1000年前相似),Sasa和Panicoideae属温带气候。至少在过去约600年中,日本南美大草原(Miscanthus sinensis)的草原每年都在燃烧。来自这项研究的Tonomine高原站点和其他四个站点的结果表明,累积土壤中的大炭通量> 10个粒子.cm(-2)y(-1)表明发生火灾的频率很高,从而导致Andropogoneae占主导地位种类。在木炭通量为2-10颗粒.cm(-2)y(-1)的土壤中,观察到了受火影响的苦竹种的优势地位,这表明该种在中等火势下(可能每几年一次)繁盛。或者更多)。在木炭通量小于1个颗粒.cm(-2)y(-1)的土壤中,火对植被没有影响,Sasa和Pleioblastus物种繁盛,而植被类型主要由气候决定条件。这些发现表明,大型木炭通量和植硅体组合表现出与年龄无关的一致关系,并且大型木炭通量与着火频率相关,因此表明着火频率决定了这些地区的植被类型。因此,累积土壤中的植物硅酸盐和木炭记录为定量了解火对过去植被格局的影响提供了背景。 (C)2015 Elsevier Ltd和INQUA。版权所有。

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